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- W1964382071 abstract "Extreme Transhimalayan (oceanic, mantle, I-type) and High Himalayan (anatectic, collision, S-type) granitoids in the Himalaya, Kashmir, and Tibet range in their original oxygen isotope composition from 6 to 7.5 and from 10 to 12.5‰ δ18OSMOW, respectively. In the sutured Paleozoic and Mesozoic orogen of the eastern Tibetan plateau, purely oceanic batholiths seem absent (Shalouli Shan 8–10‰), but High Himalayan values are matched in Dongda Shan and at Luxi. Towards the east, oceanic values are found again only on the margin of the Yangtse platform. The regional pattern of normal oxygen isotope data provides a background for anomalous feldspars (to −1‰) in Lhasa Granite and in the active geothermal system at Yangbachen, recharged by ∼6000 m a.s.l. meteoric water. For Lhasa Granite, oxygen isotope exchange paths and preliminary K–Ar dating of feldspars suggest exchange with meteoric water from over 3000 m altitude before 20 Ma ago." @default.
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- W1964382071 date "2002-12-01" @default.
- W1964382071 modified "2023-09-26" @default.
- W1964382071 title "Oxygen isotope trends and anomalies in granitoids of the Tibetan plateau" @default.
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- W1964382071 doi "https://doi.org/10.1016/s1367-9120(02)00046-9" @default.
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